GroMoPo Metadata for Upper Chaj Doab model
Authors: | |
---|---|
Owners: | gromopo_admin |
Type: | Resource |
Storage: | The size of this resource is 1.6 KB |
Created: | Feb 06, 2023 at 8:31 p.m. |
Last updated: | Feb 06, 2023 at 8:31 p.m. |
Citation: | See how to cite this resource |
Sharing Status: | Public |
---|---|
Views: | 833 |
Downloads: | 234 |
+1 Votes: | Be the first one to this. |
Comments: | No comments (yet) |
Abstract
A 3-D finite element model (Feflow) has been used for regional groundwater flow modelling of Upper Chaj Doab in Indus Basin, Pakistan. The thematic layers of soils, landuse, hydrology, infrastructure and climate were developed using Geographic Information System (GIS). The numerical groundwater flow model is developed to configure the groundwater equipotential surface, hydraulic head gradient and estimation of the groundwater budget of the aquifer. Integration of GIS with groundwater modelling and satellite remote sensing capabilities has provided an efficient way of analysing and monitoring groundwater status and its associated land conditions. The Arcview GIS software is used as additive tool to develop supportive data for numerical groundwater modelling, integration and presentation of image processing and modelling results. The groundwater behaviour of the regional model shows a gradual decline in watertable from year 1999 onward. The persistent dry condition and high withdrawal rates play an influential role in lowering down the groundwater levels. Different scenarios were developed to study the impact of extreme climatic conditions (drought/flood) and variable groundwater abstraction on the regional groundwater system. The results of the study provide useful information regarding the behaviour of aquifer in order to organize management schemes on local and regional basis to monitor future groundwater development in the area.
Subject Keywords
Coverage
Spatial


















Content
Additional Metadata
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
Comments
There are currently no comments
New Comment